The ionospheric signatures of rapid subauroral ion drifts
- Univ. of Texas, Richardson (USA)
Subauroral ion drifts (SAID) are latitudinally narrow regions of rapid westward ion drift located in the evening sector and centered on the equatorward edge of the diffuse aurora. Observations of SAID as identified by the ion drift meters on the Atmosphere Explorer C and Dynamics Explorer B spacecraft are utilized to determine their effect on the F region ion composition, their relationship to the mid-latitude trough, and their temporal evolution. At altitudes near the F peak a deep ionization trough is formed in regions of large ion drift where the O{sup +} concentration is considerably depleted and the NO{sup +} concentration is enhanced, while at higher altitudes the trough signature is considerably mitigated or even absent. SAID have been observed to last longer than 30 min but less than 3 hours, and their latitudinal width often becomes narrower as time progresses. The plasma flows westward equatorward of the SAID and becomes more westward as invariant latitude increases. Poleward of the SAID, the flow is, on average, westward throughout the auroral zone in the evening, while near midnight it becomes eastward.
- OSTI ID:
- 5223182
- Journal Information:
- Journal of Geophysical Research; (United States), Journal Name: Journal of Geophysical Research; (United States) Vol. 96:A4; ISSN 0148-0227; ISSN JGREA
- Country of Publication:
- United States
- Language:
- English
Similar Records
The auroral electrojet and global auroral features
Electron flow and visual aurora at the Harang discontinuity
Related Subjects
Ionospheric
& Magetospheric Phenomena
71 CLASSICAL AND QUANTUM MECHANICS
GENERAL PHYSICS
ATMOSPHERIC CHEMISTRY
AURORAE
AURORAL ZONES
CHEMISTRY
EARTH ATMOSPHERE
EARTH MAGNETOSPHERE
ELECTRIC FIELDS
EXPLORER SATELLITES
F REGION
ION DENSITY
ION DRIFT
IONIC COMPOSITION
IONOSPHERE
MAGNETIC BAYS
PLANETARY IONOSPHERES
PLASMA DRIFT
SATELLITES